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The Giant Okavango and Related Ma¢C Dyke Swarms, Karoo Igneous Province, Northern Botswana

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The Giant Okavango and Related Ma¢C Dyke Swarms, Karoo Igneous Province, Northern Botswana Earth and Planetary Science Letters 202 (2002) 595^606 www.elsevier.com/locate/epsl 40Ar/39Ar geochronology and structural data from the giant Okavango and related ma¢c dyke swarms, Karoo igneous province, northern Botswana B. Le Gall a;Ã, G. Tshoso a, F. Jourdan b,G.Fe¤raud b, H. Bertrand c, J.J. Tiercelin a, A.B. Kampunzu d, M.P. Modisi d, J. Dyment a, M. Maia a a UMR-CNRS 6538, Institut Universitaire Europe¤en de la Mer, 29280 Plouzane¤, France b UMR-CNRS 6526 Ge¤osciences Azur, Universite¤ de Nice-Sophia Antipolis, O6108 Nice, France c UMR-CNRS 5570, ENS et UCBL, 69364 Lyon, France d Department of Geology, University of Botswana, Gaborone, Botswana Received 25 February 2002; received in revised form 11 June 2002; accepted 13 June 2002 Abstract In NE Botswana, the Karoo dykes include a major N110‡ dyke swarm known as the Okavango giant dyke swarm (ODS/N110‡) and a second smaller set of N70‡ dykes belonging to the Sabi-Limpopo dyke swarm (SLDS/N70‡). New 40Ar/39Ar plagioclase dating of Karoo dolerites of the giant ODS/N110‡ and the SLDS/N70‡ in NE Botswana yield plateau ages between 179.6 þ 1.2 and 178.4 þ 1.1 Ma. Our data are concordant with previous 40Ar/39Ar ages for Northern Karoo dykes and lava flows exposed in western Zimbabwe. The data are tightly clustered, indicating a short-lived (179^181 Ma) flood basalt magmatism in this region. The new radiometric dates allow the definition of a diachronous Jurassic flood basalt activity in southern Africa. A significant south to north younging at the scale of the Karoo igneous province correlates with a chemical zonation from low-Ti (south) to high-Ti (north) mafic rocks. Structural measurements on the ODS/N110‡ and SLDS/N70‡ Karoo dykes of NE Botswana suggest that: (1) most of the host fractures are inherited Precambrian structures; (2) dyke emplacement occurred under unidirectional tensional stresses; (3) significant syn- and post-volcanic extensional tectonics are lacking. Combined with regional geology, these geochronological and structural data do not confirm unambiguously the triple-junction hypothesis usually put forward to support a mantle plume model for the evolution of the Karoo igneous province, prior to Gondwana breakup. ß 2002 Published by Elsevier Science B.V. Keywords: Ar-40/Ar-39; absolute ages; dike swarms; mantle plumes; Gondwana; Karoo Basin 1. Introduction The Karoo-Ferrar/Antarctica large igneous U 6 * Corresponding author. Tel.: +33-2-98-49-87-56; province (KFA-LIP hereafter) covers 6 10 2 Fax: +33-2-98-49-87-60. km and is one of the greatest continental £ood E-mail address: [email protected] (B. Le Gall). basalt provinces in the world (Fig. 1a). It is linked 0012-821X / 02 / $ ^ see front matter ß 2002 Published by Elsevier Science B.V. PII: S0012-821X(02)00763-X EPSL 6302 16-9-02 596 B. Le Gall et al. / Earth and Planetary Science Letters 202 (2002) 595^606 Fig. 1. Major Precambrian and Karoo structural features of West Gondwana. (a) Distribution of continental £ood basalt and re- lated intrusive rocks of the Karoo-Ferrar/Antarctica large igneous province in a pre-drift Gondwana reconstruction. 1, exposed complexes; 2, extrapolated magmatic rocks; 3, inferred magmatic units beneath ice cover in western Antarctica. HTP and LTP, high- and low-Ti tholeiitic province, respectively. (b) Karoo tectono-magmatic framework of southern Africa. 1, magmatic com- plexes with 1a, £ood basalt; 1b, dykes and sills; 1c, eruptive centres; 2, sedimentary basins. C, Chilwa; L, Lesotho; LDS, Le- bombo dyke swarm; MTZ, Mozambique thinned zone; N, Nuanetsi; ODS, Okavango dyke swarm; ORDS, Olifants River dyke swarm; RRS, Rooi Rand Suite; SBDS, South Botswana dyke swarm; SLDS, Sabi-Limpopo dyke swarm; SLeDS, South Lesotho dyke swarm; SMDS, South Malawi dyke swarm; ZF, Zoetfontain fault. (c) Major basement boundaries in southern Africa. 1, palaeozoic belt; 2, proterozoic belts; 3, craton; 4, dyke swarms; 5, suture lines. EACF, East African coastal fault; GD, Great Dyke; MSZ, Magogaphate shear zone; PT, Pongola rift trend; VT, Venterdorp rift trend. to the initial Jurassic breakup of Gondwana. The largely documented with emphasis on the petrol- African section of this LIP, the Karoo igneous ogy of igneous rocks [1], thermo-mechanical and province, consists of £ood basalts, sills and giant geotectonic evolution related to either mantle dyke swarms that together cover more than plume or subduction processes [2,3]. However, 3U106 km2 in southern Africa (Fig. 1b). The evo- limited ¢eld structural data and precise geochro- lution of the Karoo igneous province has been nological data (e.g. [4,5] have been integrated to EPSL 6302 16-9-02 B. Le Gall et al. / Earth and Planetary Science Letters 202 (2002) 595^606 597 Fig. 2. The Karoo dyke system in NE Botswana. (a) Simpli¢ed geological map showing the location of the N110‡ (Okavango) and N70‡ (Sabi-Limpopo) dyke swarms. The studied areas, including the Shashe reference section, Tsetsebjwe (Ts) and Tuli (THG), as well as isolated dated samples are shown. 1, regional envelop of the N110‡ and N70‡ dyke swarms; 2, £ood basalt; 3, Karoo basins; 4, Precambrian basement with 4a, dominantly gneissic rocks; 4b, granites; 5, major extensional faults. F, Francis- town; G, Gulubane; MF, Magogaphate fault; ODS, Okavango dyke swarm; T, Tonotha. (b) Location of dated rocks along the Shashe section. The distribution of dykes is according to published geological maps of the Geological Survey of Botswana. Loca- tion of Fig. 3 is also shown. constrain the geotectonic models. Furthermore, interpretation: (1) the temporal relationships be- though ma¢c dyke swarms are known to be cru- tween the various dyke swarms is not yet estab- cial indicators for mantle dynamics and crustal lished, and (2) the inherited or newly formed ori- palaeostress regimes, precise geochronological gin of the involved fractures was not documented. and structural information related to the giant This paper is focused on: (1) the giant N110‡ Okavango dyke swarm are still missing. Fig. 1b Okavango dyke swarm (ODS/N110‡) which rep- indicates that the Karoo intrusive complex is resents one of the greatest ¢ssural intrusive com- dominated by four di¡erent dyke sets, namely plexes in the world [9]. It forms a 1500-km-long the Okavango (N110‡), Sabi-Limpopo (N70‡), and 100-km-wide tectono-magmatic structure ex- Lebombo (N-S) and Olifants River (N20^40‡) sys- tending from Nuanetsi in western Zimbabwe tems. These four dyke arrays converge towards through northern Botswana up to northern Na- the Nuanetsi area, in southern Zimbabwe, which mibia (Fig. 1b). (2) The N70‡ dyke swarm (SLDS/ is considered to be a rift triple-junction formed N70‡) exposed south of the ODS/N110‡ and cor- above a mantle plume [2,6^8]. However, the fol- responding to the SW tip of the Sabi-Limpopo lowing critical issues were not addressed in that dyke system [10]. Except for one 40Ar/39Ar EPSL 6302 16-9-02 598 B. Le Gall et al. / Earth and Planetary Science Letters 202 (2002) 595^606 Fig. 3. Structural features of the Karoo ODS/N110‡ swarm and its Proterozoic basement host-rocks (see location in Fig. 2b). (a) Vertical attitude of a N70‡ segmented dyke at the Shashe Dam (sample BOT/0055). (b) Small-scale segmentation of a N110‡ dyke (10 cm thick) caused by a basement-related N70‡ brittle fracture. (c) N70‡ brittle shear planes in orthogneiss from the Shashe Dam-Tonotha area. (d) N70‡ granite veins and epidote-¢lled cracks dextrally o¡set by a N110‡ (dyke-parallel) basement fault, Shashe Dam area. whole-rock age determination on a ma¢c dyke to present ¢eld structural observations for both from the external part of the swarm [11], the dyke systems; and (3) to integrate our data in ODS/N110‡ and SLDS/N70‡ have never been the regional framework in order to generate con- dated and their structural setting never been fully strained interpretations on the rift triple-junction documented. model. The ODS/N110‡ has been variously interpreted as: (1) a failed arm of a triple rift junction above a starting mantle plume which led to the breakup 2. Geological framework and structural analysis of Gondwanaland [2,12,13]; (2) the result of a plume impinging a subducting lithosphere [3]; The Pre-Kalahari basement is well exposed in (3) a South Atlantic ocean-related magmatism NE Botswana and primarily comprises foliated emplaced along a Cretaceous continental trans- Archaean rocks of the Zimbabwe craton and verse fracture [14]. Limpopo belt and unconformably overlying Per- The objectives of this paper are: (1) to present mo-Jurassic Karoo sedimentary and volcanic se- new 40Ar/39Ar ages on plagioclases from N110‡ quences of the Central Kalahari basin and Tuli and N70‡ dyke sets in northern Botswana; (2) half-graben [15^18] (Figs. 1b and 2a). EPSL 6302 16-9-02 B. Le Gall et al. / Earth and Planetary Science Letters 202 (2002) 595^606 599 The average length of individual dykes within 3. Geochronology the ODS/N110‡ is 10 km with a mean N110‡ azi- muth parallel to the swarm trend (Fig. 2b). The 3.1. Sample description and analytical procedures highest exposed dyke density occurs in the Fran- cistown area which is drained by the Shashe Riv- Ten samples of ma¢c dykes intruding into Ar- er. The nearly unbroken exposures along the chaean gneissic granites (nine samples) and Karoo Shashe River allow a complete sampling of all sediments (one sample) in NE Botswana were se- the dykes of the ODS/N110‡ within a ca. 80- lected for 40Ar/39Ar dating. They are representa- km-long continuous section, at high angle to the tive of both the ODS/N110‡ (BOT/03-10A-17-19- swarm trend (Fig.
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